The transfer of heat and water vapor from the ocean to the air
above it depends on a disequilibrium at the interface of the water and the air.
Within about a millimeter of the water, air temperature is close to that of the
surface water, and the air is nearly saturated with water vapor. But the
differences, however small, are crucial, and the disequilibrium is maintained by
air near the surface mixing with air higher up, which is typically appreciably
cooler and lower in water-vapor content. The air is mixed by means of turbulence
that depends on the wind for its energy. As wind speed increases, so does
turbulence, and thus the rate of heat and moisture transfer. Detailed
understanding of this phenomenon awaits further study. An interacting—and
complicating—phenomenon is wind-to-water transfer of momentum that occurs when
waves are formed. When the wind makes waves, it transfers important amounts of
energy—energy that is therefore not available to provide turbulence.
For the following question, consider each of the choices separately and
select all that apply. According to the passage, wind over the
ocean generally does which of the following
A. Causes relatively cool, dry air to come into proximity with the ocean
surface.
B. Maintains a steady rate of heat and moisture transfer between the ocean
and the air.
C. Causes frequent changes in the temperature of the water at the ocean’s
surface.